Evidence for low sulfate and anoxic deep waters in early Cambrian
The role of environmental change as a significant force driving biological evolution during the Ediacaran–Cambrian transition remains a subject of extensive debate. In this study, we present high-resolution C-isotope data of organic matter (δ13Corg) and multiple S-isotope compositions of pyrite (δ34...
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Published in | Palaeogeography, palaeoclimatology, palaeoecology Vol. 648; p. 112281 |
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Main Authors | , , , , , , , , |
Format | Journal Article |
Language | English |
Published |
Elsevier B.V
15.08.2024
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Subjects | |
Online Access | Get full text |
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